It depends if it is an isotope or not
40-Argon is formed by the radioactive decay of 40-Potassium. 40-Argon is stable so it could have been created from the potassium 4 billion years ago or yesterday; or even 5 nanoseconds ago.
The radioactive decay of potassium 40 produces in argon 40. The proportion of these two isotopes in rocks permit their age to be calculated.
Argon occurs as a result of the radioactive decay of 40K ( potassium 40 ) Potassium is common on Earth; about 1/60th of it's crust is potassium. Naturally occurring potassium is a mixture of three isotopes. Almost all of it is 39K and 41K, both of which are stable. About 1 atom in 10,000 is 40K, which is unstable. It has a very long half-life, >109 years; it decays to 40Ar which is stable.
10 grams... If the half-life is 100 years, that means after 100 years, half the original mass remains. After another 100 years, the mass is halved again. 40/2=20... 20/2=10.
Radio active parent elements decay to stable daughter elements i.e. the radio active parent Potassium 40 decays to Argon 40 Each radioactive isotope has it's own half life A half life is the time it takes for the parent radioactive element to decay to a daughter product, Potassium 40 decays to Argon 40 with a half life of 1 1/4 billion years. Therin lies the problem of storing nuclear waste
It depends if it is an isotope or not
It is 2.5 billion years.
1.89 seconds (:
Argon-40 Naturally occurring K-40 with a half-life of 1.25×109 years, decays to stable Ar-40 (11.2%) by electron capture or positron emission.
The isotope potassium-40 decays into argon-40 at a predictable rate. By measuring the ratio of the two present in a rock, we can work out how long it is since the rock was formed from magma. where t is the elapsed time, t1/2 is the half life of the decay, Kf is the amount of potassium -40 left in the sample, and Arf is the amount of argon-40 present. Measuring the quantities of the isotopes is very easy with a mass spectrometer.
The half life of potassium 40 is 1.3 billion years.
The half life of potassium 40 is 1.3 billion years.
Some of Potassium-40 decays into Argon-40 at a half - life of 1.25 x10^9 years. [About 11% of K40 decays by this method, the other 89% decays into Ca40 which is stable. ] The Argon-40 remains trapped in the crystal matrix, and may with care be recovered. So it is just a matter of determining in the laboratory the proportions of each of the materials, and applying the half-life calculations. [A 70kg person has around 4000 K40 nuclei decaying each second!]
neutrons = 22 (for the most stable isotope of argon, Ar-40)
The element Argon has 8 Isotopes argon-35, argon-36, argon-37, argon-38, argon-39, argon-40, argon-41 and argon-42.The stable isotopes of argon are:argon-36, 0.34%argon-38, 0.06%argon-40, 99.60%Of the radioactive isotopes argon-39 has the longest halflife at about 260 years, all the others have halflives measured in days or much less.
Argon-40, the most common isotope is formed by the radioactive decay of potassium-40.